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Three dimensional numerical modeling of tsunami related internal gravity waves in the Hawaiian atmosphere

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Figure

Fig. 1. Left: schematic representation of tsunami-related-IGW propagation with its vertical VZ-IGW =kzkh2 N2ωD2and horizontal VH-IGW =kh N2(D−kh2)ωD2group velocities, where kz and kh are the vertical and horizontal k-vector, g the gravity, N the Brunt-V¨ai
Fig. 3. (a) IGW imaged by the 630.0-nm ground-based airglow camera located on the Haleakala Volcano on Maui, Hawaii, at 13:20 UT

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